At some points, the oceanic crust bends downward and forms a deep-ocean trench. Then the oceanic crust sinks back into the mantle through a process called subduction.
The descending oceanic crust starts to melt. This is due to the presence of volatiles in the crust that reduce its melting point as well as the increased temperatures with depth. This can be thought of as a form of recycling of the crust.
subdution
Deep ocean trenches are typically the evidence of the collision of tectonic plates. This collision is often known as subduction.
Deep ocean trenches are associated with subduction zones where an ocean plate descends into the asthenosphere. The Ocean plate is heavier than a Continental plate which causes the Ocean plate to slide beneath the Continental plate. As the Ocean plate descends, a deep ocean trench is formed.
Sea Floor spreading has to do with the crust forming at ocean ridges and being destroyed at deep sea trenches.
they occur because a big japaneese fart master sat on the ocean and made it have a bigger crack than his. the crack goes deep under the land it is pushed under and forms a barrel cave for bugs to sit in while they eat at the ground.. heheh
the Pacific Ocean with a few in the Indian Ocean.
what happens is the ocean floor does not just keep spreading.instead, it sinks beneath deep underwater canyons called deep- ocean trenches
subdution
Deep ocean trenches form
Deep ocean trenches are deep slits in the middle of the ocean. The pressure inside these trenches is unbearable. long, curved valleys along the edges of the ocean basin
Giant squid primarily live in deep ocean trenches.
Trenches
They live in deep trenches in the ocean.
At deep-ocean trenches, subduction allows part of the ocean floor to sink back into the mantle. The ocean floor does not just keep spreading. Instead, it sinks beneath deep underwater canyons called deep-ocean trenches. Where there are trenches, subduction takes place.
At deep-ocean trenches, subduction allows part of the ocean floor to sink back into the mantle. The ocean floor does not just keep spreading. Instead, it sinks beneath deep underwater canyons called deep-ocean trenches. Where there are trenches, subduction takes place.
Deep ocean trenches are typically the evidence of the collision of tectonic plates. This collision is often known as subduction.
Some ocean trenches can be as deep as 10,971 m (35,994 ft).
a deep-ocean trench is a portion of the earth crust